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- W2188549609 abstract "Borehole temperatures in Hole 395A were continuously logged during Leg 109, over 10 years after the hole was drilled during Leg 45 and about 5 years after temperatures in the hole were previously measured during Leg 78B. The more precise Leg 109 data are basically consistent with temperatures measured during Leg 78B, except at intermediate depths of 300-500 mbsf. Temperatures measured during Leg 109 indicate a vigorous flow of ocean bottom water down the 112 m of casing and into the permeable upper basement, at a rate virtually undiminished since Leg 78B. The temperature gradient in the sediments was measured at the nearby Hole 395C, allowing the rate of flow down Hole 395A to be estimated at about 10-100 m/hr. The fine-scale structure in temperature gradients in Hole 395A indicates that the water outflow occurs predominantly in the basement above 300 mbsf, with additional outflow zones between 430 and 530 mbsf. Below 450 mbsf, the gradient profile is affected by flow within the borehole, but indicates predominantly conductive heat transfer. The temperature gradient in the deeper section is consistent with a heat flow of about 200 mW/m2, close to the value predicted for the 7.3-m.y.-old crust at the site." @default.
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- W2188549609 date "1990-10-01" @default.
- W2188549609 modified "2023-10-05" @default.
- W2188549609 title "Temperature Measurements at Site 395, ODP Leg 109" @default.
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- W2188549609 doi "https://doi.org/10.2973/odp.proc.sr.106109.144.1990" @default.
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